EGU2020-8371
https://doi.org/10.5194/egusphere-egu2020-8371
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

A Parametrization for Triad Interactions of Internal Gravity Waves in Varying Background Flows for WKBJ Ray-Tracing Methods

Georg Sebastian Voelker1, Triantaphyllos Akylas2, and Ulrich Achatz1
Georg Sebastian Voelker et al.
  • 1Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences, Theory of Atmospheric Dynamics and Climate, Frankfurt/Main, Germany (voelker@iau.uni-frankfurt.de)
  • 2Massachusetts Institute of Technology

Internal gravity waves are a well known mechanism of energy transport in stratified fluids such as the atmosphere and the ocean. Their abundance and importance for various geophysical processes like ocean mixing and momentum deposition in atmospheric jets are widely accepted. While resonant wave-wave interactions of monochromatic disturbances have received intensive study, little work has been done on triad interactions between wave trains that are modulated by a variable mean flow.

Using the method of multiple scale asymptotics we consider a weakly non-linear Boussinesq WKBJ theory for interacting gravity wave trains propagating through a finite amplitude background flow. Consequently the wave trains are allowed to spectrally pass through resonance conditions and exchange energy when sufficiently close to resonance. We find a global optimal threshold for the deviation from resonance and derive a corresponding parametrization for the triad interaction applicable to ray tracing schemes.

We test the theory with idealized simulations in which two wave trains generate a third by passing through resonance in a sinusoidal background shear flow with varying vertical scales. Comparing WKBJ simulations with wave resolving large eddy simulations we find qualitative and quantitative agreement. Furthermore we assess the impact of the strength of the modulation as well as the effect of the wave amplitudes on the energy exchange between the interacting wave triad.

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Presentation version 1 – uploaded on 03 May 2020
  • CC1: Comment on EGU2020-8371, Paul Pukite, 10 May 2020

    Thanks for answering my question on triad waves wrt Bruce Sutherland's work during the chat. I had written a blog post on the topic recently https://geoenergymath.com/2020/04/06/triad-waves/

    The role of a triad in transferring energy from waves of different wavelengths makes sense to me and may be a mechanism in creating the set of standing waves along the equator, i.e. ENSO and the shorter tropical instability waves.